Liu Jie, Ji Yu-He, Zhou Guang-Sheng, Zhou Li, Lyu Xiao-Min, Zhou Meng-Zi
School of Geo-Science and Technology, Zhengzhou University, Zhengzhou 450001, China.
Joint Laboratory of Eco-Meteorology, Chinese Academy of Meteorological Sciences and Zhengzhou University, Zhengzhou 450001, China.
Ying Yong Sheng Tai Xue Bao. 2022 Jun;33(6):1533-1538. doi: 10.13287/j.1001-9332.202206.025.
Qinghai-Tibet Plateau is a "climate change laboratory" for China and the world. Driven by climate change, net primary productivity (NPP) in the Qinghai-Tibet Plateau has significant variations. Using the data of normalized difference vegetation index, digital elevation, annual precipitation, and annual temperature, we explored the temporal and spatial variation characteristics of NPP and its correlation with climate factors on the Qinghai Tibet Plateau from 2000 to 2020. The results showed that NPP of the Qinghai-Tibet Plateau increased significantly from 2000 to 2020, with an increase rate of 1.67 g C·m·a. The NPP was significantly positively correlated with temperature and precipitation. The climate trend of warming and wetting was an important driving force to promote the significant increase of NPP. The increases of NPP would continue if the climate become warmer and wetter.
青藏高原是中国乃至世界的“气候变化实验室”。在气候变化的驱动下,青藏高原的净初级生产力(NPP)有显著变化。利用归一化植被指数、数字高程、年降水量和年气温数据,我们探讨了2000年至2020年青藏高原NPP的时空变化特征及其与气候因子的相关性。结果表明,2000年至2020年青藏高原NPP显著增加,增加速率为1.67 g C·m·a。NPP与气温和降水显著正相关。气候暖湿化趋势是推动NPP显著增加的重要驱动力。如果气候变得更暖湿,NPP的增加将持续。